2 edition of High-precision temperature logging at GISP2, Greenland, May 1992 found in the catalog.
Published 1995 by Administrator in U.S. Dept. of the Interior, U.S. Geological Survey
Distributed to depository libraries in microficheShipping list no.: 97-0273-MMicrofiche. [Denver, Colo. : U.S. Geological Survey, 1995] 1 microfiche
|Statement||U.S. Dept. of the Interior, U.S. Geological Survey|
|Publishers||U.S. Dept. of the Interior, U.S. Geological Survey|
|The Physical Object|
|Pagination||xvi, 68 p. :|
|Number of Pages||45|
|2||U.S. Geological Survey open-file report -- 95-490|
|3||Open-file report -- 95-490|
nodata File Size: 2MB.
But suddenly he meets a man with the face of his deceased as Marmion still thinks enemy Wilton.
The Last Glacial Maximum, the Climatic Optimum, the Medieval Warmth, the Little Ice Age, and a warm period at 1930 A. These two logs compare with each other quite well. Initial measurements of CO 2 in air bubbles of the GISP2 core by the measurement of electrical conductivity, chemistry and insoluble particles providing evidence of local High-precision temperature logging at GISP2 e. This night Marmion is unable to sleep and goes for a ride to calm himself.
The uncertainty of depth measurements is less than 250 ppm.
Quantification of fluxes of soluble ionic species attributable to these processes has been one objective of 1993 sampling. The sensor's true resistance R s is then converted to temperature T using a 4—term calibration function similar to the often used 3—term Steinhart—Hart equation. The control panel and instrument package Figure 5 for the PICO deep drill were developed at the University of Nebraska-Lincoln. 482-485, 1994 Polar ice stratigraphy from laser-light scattering: Scattering from meltwater.
7 foot long in one unbroken piece. With the set of calibrations used in this project, the uncertainty of measured temperatures is smaller than 3. Greenland obtained from the deep core were divided on the basis of volume and analytical requirements Figure 9.
37 Currently reading Published 1885 by in. Science A Monte Carlo inverse method has been used on the temperature profiles measured down through the Greenland Ice Core Project GRIP borehole, at the summit of the Greenland Ice Sheet, and the Dye 3 borehole 865 kilometers farther south. and spectral models Bolzan, pers.
3 mK compared to absolute standards, and less than 2 mK for temperature differences along the borehole.
The bulk of these efforts have taken place at the remote, solar powered, clean sampling site ATM 29 km southwest of the GISP2 drill camp.
One of the most dramatic climate events observed in marine and ice core records is Younger :Dryas YD , a return to near glacial conditions that punctuated the last glaciation Figure 14.
The magnitudes of these additional uncertainties are still being assessed but are generally less than 10 mK.